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- W2182099151 abstract "The D-region of the ionosphere is remotely probed by ground-based radar. The method used is referred to as the partial reflection-drift experiment. The partial-reflection experiment is used to determine the horizontal-drift velocity of ionized irregularities in the ionosphere. If a point radio source is used, the stratified irregularities produce a diffraction pattern over the ground. By sensing this diffraction pattern with a minimum of three antennas the horizontal-drift velocity can be computed. To determine the horizontal-drift velocity of the ionosphere it is necessary to illuminate the ionosphere with a single radio-wave point source. When this is done a diffraction pattern is formed from the ionosphere irregularities in the D-region. The E and F region of ionosphere is studied using the ionospheric data from archives of ionospheric station. The ionospheric datas were used for training neural networks (NNs) to predict the parameters required to produce the final profile. The NNs have been trained to predict the individual ionospheric characteristics and coefficients that were required to describe the profile. 1. Objective" @default.
- W2182099151 created "2016-06-24" @default.
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- W2182099151 date "2009-01-01" @default.
- W2182099151 modified "2023-09-27" @default.
- W2182099151 title "STUDY OF D, E AND F REGIONS OF IONOSPHERE" @default.
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